Millions of years
Plants and animals can become fossils in sedimentary rocks because these rocks are formed from layers of sand, silt, and clay that accumulate over time, preserving the remains. As sediment builds up, it can bury dead organisms and protect them from decay, leading to the formation of fossils. The slow process of sedimentation helps in the preservation of details of the organisms, allowing researchers to study past life forms.
Seed plants carry out long distance reproduction by animals, rain, wind, or pollen.
Seed plants carry out long distance reproduction by animals, rain, wind, or pollen.
No current plants, but some fossil imprints are of long dead plants (usually from about 1/4 billion yeas ago).
Sedimentary rock forms when material from dead plants and animals, along with other debris, is compacted and cemented over time. This process creates rock layers rich in organic material, such as coal or limestone, from the remains of living organisms.
The animal or plants needs to be covered in a sedimentary silt or mud, for a very long time.
The plants from long ago are like animals of long ago in a couple of ways. Both have survived through time.
Long horned grasshoppers have a very different diet than other grasshoppers. In addition to plants, long horned grasshoppers eat other insects and feed off of dead animals.
humans
Rocks that form from dead plants and animals that have been compressed are called sedimentary rocks. Examples include coal, which forms from compressed plant matter, and limestone, which can contain compressed remains of marine organisms. This process of transformation over time is known as diagenesis.
Carbohydrates are used as an energy source for plants. They become crucial after a long hard winter where photosynthesis has not taken place. In this case, the plants rely on carbohydrate stores to provide the energy they need to produce new growth.
Plants and animals can become fossils in sedimentary rocks because these rocks are formed from layers of sand, silt, and clay that accumulate over time, preserving the remains. As sediment builds up, it can bury dead organisms and protect them from decay, leading to the formation of fossils. The slow process of sedimentation helps in the preservation of details of the organisms, allowing researchers to study past life forms.
Fossil fuels are made up of dead animals and plants and over a long period of time, the decayed plants and animal remains are compressed together with dirt.Over millions of years they will form coal.
The act of stuffing dead animals, mounting them, and placing them on display is called taxidermy. Somebody who practices taxidermy is called a taxidermist.
Well, most of the time geologists find fossils of plants and animals, and then study them to find out how long ago the plant(or animal) lived.
1000 years
Seed plants carry out long distance reproduction by animals, rain, wind, or pollen.